Zhao Shengrong, Pei Haiying. Preprocessing precipitation in objective quantitative forecast. J Appl Meteor Sci, 2007, 18(1): 21-28.
Citation: Zhao Shengrong, Pei Haiying. Preprocessing precipitation in objective quantitative forecast. J Appl Meteor Sci, 2007, 18(1): 21-28.

Preprocessing Precipitation in Objective Quantitative Forecast

  • Received Date: 2005-09-13
  • Rev Recd Date: 2006-06-26
  • Publish Date: 2007-02-28
  • Quantitative precipitation forecast is much difficult in objective forecast. It is because that the precipitation is not a continuous variable, either not a normal distribution variable. Except that the precipitation has an obviously different characteristic to other elements that zero precipitation include many different situations. For example, black clouds blot out the sky but precipitation amount is zero. There are not many clouds on the sky and precipitation amount is also zero. These two situations are different, but the difference is not exhibited in the amount of precipitation. So the effectiveness of the forecast model is affected.Preprocessing has important effects on forecast results. For the purpose of improving quantitative precipitation forecast effectiveness, a reasonable preprocessing scheme needs to be developed. Precipitation observation is preprocessed using relative humidity before modeling. The amount of precipitation is changed to different negative values when relative humidity is smaller than usual and precipitation amount equals zero. Based on the summer data of 2003 and 2004, forecast model of preprocessing precipitation and direct precipitation are developed respectively.BP network method is used in the study, which is a kind of artificial neural network. The BP network is a back propagation network. It contains input layer, implicit layer and output layer. There can be one or more implicit layers on the BP network. Joint on the implicit layer is named implicit node. Input signals propagate to implicit nodes. Then signals of implicit nodes propagate to the next layer after the disposal of weights and operating functions. At last, the value on the output nodes is gotten. BP networks can be considered as a nonlinear projection from input layer to output layer. Sigmond function is always taken as the operating function. Network weights of different nodes are obtained by training. The BP algorithm is used in training process.Predictors are corresponding to precipitation amount forecast of operational global model of China National Meteorological Center, operational models of German Meteorological Administration and Japan Meteo rological Agency. In order to avoid errors caused by interpolating, to every model, precipitation forecast on four grids around the stations are used as predictors instead of interpolated model precipitation forecasts at stations.Test of different forecast results during 2005 summer of Beijing and other 5 stations indicate that precipitation forecasts are improved after preprocessing. Especially absent forecasts are reduced. So it can be concluded that this reprocessing method is simple and effective. But it only provides some ideas. In real settings, different element also can be used to reprocess precipitation amount according to different areas or different seasons in a year.
  • Fig. 1  TS score of 36 h light rain forecast averaging from June to August in 2005

    Fig. 2  No-hitting rate of 36 h light rain forecast averaging from June to August in 2005

    Fig. 3  Fault-hitting rate of 36 h light rain forecast averaging from June to August in 2005

    Fig. 4  Forecast bias of 36 h light rain forecast averaging from June to August in 2005

    Fig. 5  TS score (a) and fault-hitting rate (b) of 36 h light rain forecast averaging from June to August in 2005

    Fig. 6  TS score of 36 h moderate rain (a) and heavy rain (b) forecast averaging from June to August in 2005

  • [1]
    刘还珠, 赵声蓉, 陆志善, 等.国家气象中心气象要素的客观预报———MOS系统.应用气象学报, 2004, 15 (2): 181-191. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20040223&flag=1
    [2]
    胡江林, 涂松柏, 冯光柳.基于人工神经网络的暴雨预报方法探讨.热带气象学报, 2003, 19 (4): 423-428. http://www.cnki.com.cn/Article/CJFDTOTAL-RDQX200304009.htm
    [3]
    刘爱鸣, 潘宁, 邹燕, 等.福建前汛期区域暴雨客观预报模型研究.应用气象学报, 2003, 14 (4): 420-429. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20030452&flag=1
    [4]
    赵声蓉.多模式温度集成预报.应用气象学报, 2005, 17 (1): 52-58. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20060109&flag=1
    [5]
    张万诚, 解明恩.奇异值分解方法对降水的预测试验.高原气象, 2002, 21(1): 103-107. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX200201016.htm
    [6]
    宋海鸥, 王永红, 顾善齐, 等.应用K指数和TOT指数制作江苏中期降水预报的试验.气象科学, 2002, 22(2): 242-246. http://www.cnki.com.cn/Article/CJFDTOTAL-QXKX200202015.htm
    [7]
    陈力强, 韩秀君, 张立群.基于MM5模式的站点降水预报释用方法研究.气象科技, 2003, 31 (5): 268-272. http://www.cnki.com.cn/Article/CJFDTOTAL-QXKJ200305002.htm
    [8]
    龚佃利, 王以琳, 谢考宪.山东飞机增雨降水区分级预报方法研究.应用气象学报, 2001, 12 (增刊): 139-145. http://www.cnki.com.cn/Article/CJFDTOTAL-YYQX2001S1017.htm
    [9]
    曹晓岗.利用T106数值预报产品作江西暴雨动态落区预报.江西气象科技, 1998, 21 (1): 2-5. http://www.cnki.com.cn/Article/CJFDTOTAL-HXQO199801001.htm
    [10]
    赵振宇, 徐用懋. 模糊理论和神经网络的基础与应用. 北京: 清华大学出版社; 南宁: 广西科技出版社, 1996.
    [11]
    赵声蓉. 多模式降水集成预报∥章国材, 谢璞. 奥运气象保障技术研究. 北京: 气象出版社, 2004.
  • 加载中
  • -->

Catalog

    Figures(6)

    Article views (3294) PDF downloads(1637) Cited by()
    • Received : 2005-09-13
    • Accepted : 2006-06-26
    • Published : 2007-02-28

    /

    DownLoad:  Full-Size Img  PowerPoint